11 testing shear strength and deformation along discontinuities in salt

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Testing Shear Strength and Deformation along Discontinuities in Salt 8 th US/German Workshop on Salt Repository Research, Design, and Operation Steven R. Sobolik, Sandia National Laboratories, Albuquerque, New Mexico, USA Stuart Buchholz, RESPEC, Rapid City, South Dakota, USA Middelburg, The Netherlands September 5-7, 2017 Sandia National Laboratories is a multi-mission laboratory managed and operated by National Technology and Engineering Solutions of Sandia LLC, a wholly owned subsidiary of Honeywell International Inc. for the U.S. Department of Energy’s National Nuclear Security Administration under contract DE-NA0003525. This research is funded by WIPP programs administered by the Office of Environmental Management (EM) of the U.S. Department of Energy. SAND2017-9197C

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Page 1: 11 Testing Shear Strength and Deformation along Discontinuities in Salt

Testing Shear Strength and Deformation along Discontinuities in Salt

8th US/German Workshop on Salt Repository Research, Design, and Operation

Steven R. Sobolik, Sandia National Laboratories, Albuquerque, New Mexico, USA

Stuart Buchholz, RESPEC, Rapid City, South Dakota, USA

Middelburg, The Netherlands

September 5-7, 2017

Sandia National Laboratories is a multi-mission laboratory managed and operated by

National Technology and Engineering Solutions of Sandia LLC, a wholly owned subsidiary

of Honeywell International Inc. for the U.S. Department of Energy’s National Nuclear

Security Administration under contract DE-NA0003525. This research is funded by WIPP

programs administered by the Office of Environmental Management (EM) of the U.S. Department of Energy. SAND2017-9197C

Page 2: 11 Testing Shear Strength and Deformation along Discontinuities in Salt

Test Proposal

Purpose:

To measure, evaluate and quantify effects of shear displacement along a bedding interface or clay seam on shear and fracture strength of the interface and accompanying salt.

Evaluate bedded salt modeling concerning deformation, failure at seams, and bedding planes.

Expected outcome:

Improve understanding of shear stresses and strains on bedding interfaces that can be translated to current geomechanical and performance assessment models.

Reduce uncertainty. 2

Page 3: 11 Testing Shear Strength and Deformation along Discontinuities in Salt

Test Phases

Scoping laboratory tests of shear across interfaces using controlled samples (blocks of different materials such as anhydrite and halite) and samples obtained from the field (halite with included clay seam) – Autumn 2017.

Numerical modeling of laboratory results to develop appropriate shear friction/fracture models – 2017-2018.

Underground tests in alcove wall with clay seam or similar interface – 2018 (maybe).

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Page 4: 11 Testing Shear Strength and Deformation along Discontinuities in Salt

Discontinuities in salt

Influence of nonhomogeneities in repository performance identified as 1 of 4 key areas of the research agenda

Examples include bedding interfaces, boundary shear planes, joints, and seams of non-halite material such as anhydrite

Does shear strain create a permeable flow path along an interface or premature salt failure?

Little existing lab or in situ data to characterize shear strength of salt interface and effects of shear on interface displacement and permeability 4WIPP Stratigraphy

Page 5: 11 Testing Shear Strength and Deformation along Discontinuities in Salt

Discontinuities in salt (Popp, Van Sambeek)

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Page 6: 11 Testing Shear Strength and Deformation along Discontinuities in Salt

Early test proposed for WIPP

Munson & Matalucci (1983) proposed in situ test with direct shear across clay seam.

1 X 1-m block in wall containing representative clay seam would be isolated by cutting around it in place in one of the drifts.

Flatjacks installed in slots cut around the block to apply shear and normal stresses.

Displacements along and across the seam would be measured as function of applied stress.

This proposed test never occurred.

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Page 7: 11 Testing Shear Strength and Deformation along Discontinuities in Salt

Laboratory testing in 2017

Test description: Series of laboratory tests to begin in late 2017 to be used in conjunction with WIPP, WEIMOS modeling exercises.

Test plan written, completed WIPP QA reviews 7/27/2017.

Contract modification between SNL, RESPEC in process, pending DOE requirements for WIPP; NEPA checklist completed 8/7/2017

Plan to obtain cores for up to 33 test samples from New Mexico potash/salt mines: 30 cm diameter, 56 cm length cores cut vertically from floor

Cores to contain clay seam identified from further uphill in drift

Test samples cut from cores will be 10-cm cylinders or square blocks

Seam size no greater than 2.5 cm; or interface between distinct layers

Material next to seam/interface – halite, polyhalite, anhydrite

Asperity characteristics?7

Page 8: 11 Testing Shear Strength and Deformation along Discontinuities in Salt

Laboratory testing goals

Laboratory shear tests similar to those on carnalite and salt performed in 2007 (Minkley & Mühlbauer); test results were used for model development.

2017 laboratory tests require following: 10-cm samples, with existing or fabricated interface

6.9-20.7 MPa stress capacity both in axial (compression) and shear loading

Fixed normal stress for most tests; fixed normal displacement another option

Variable shear velocity to evaluate onset of fracture/slip

RESPEC direct shear machine (Capacity for up to 15-cm cube samples, 130 kN capacity, shear velocities 0.25-5 mm/min.)

Analysis plan in process (Reedlunn) to develop constitutive, numerical model for shear slip in seams from results of 2017 lab tests. 8

Page 9: 11 Testing Shear Strength and Deformation along Discontinuities in Salt

Shear Test Setup Similar to Minkley test setup

RESPEC direct shear machine

Eliminates bending force due to shear (box that holds specimen)

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Weight balanced upper shear box

Shear load ram vertically aligned with midheight of interface gap

Pinned linkage

Spherical seat

Rollered contact for normal load on upper shear box

Normal load ram centered with centerline of specimen

Page 10: 11 Testing Shear Strength and Deformation along Discontinuities in Salt

Shear Test Setup (Actual Test)

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Weight balanced upper shear box

Shear load ram aligned with centerline of interface gap

Pinned linkage

Rollered normal load application to upper shear boxCenter of pressure remains aligned with center of bottom box

Page 11: 11 Testing Shear Strength and Deformation along Discontinuities in Salt

German shear test - velocity

Dependence of the friction on the velocity of the running shear process is plotted here.

At high shear velocities, adhesive friction resistance must be overcome before a loss of strength appears. Under such conditions a significant drop in shear stress occurs.

At low shear velocities, no additional resistance of adhesive friction develops as in the case of a quick movement and, thus, cohesion is maintained.

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0

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0 1 2 3 4 5 6

shea

rst

ress

[

MP

a]

shear displacement us [mm]

0

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0 1 2 3 4 5 6

shea

rst

ress

[

MP

a]

shear displacement us [mm]

Result of computation

Laboratory test result

Result of computation

Laboratory test result

v = 0.002 mm/s

v = 0.000005 mm/s

0

2

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shea

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shear displacement us [mm]

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0 1 2 3 4 5 6

shea

rst

ress

[

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shear displacement us [mm]

Result of computation

Laboratory test result

Result of computation

Laboratory test result

0

2

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0 1 2 3 4 5 6

shea

rst

ress

[

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shear displacement us [mm]

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0 1 2 3 4 5 60 1 2 3 4 5 6

shea

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[

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shear displacement us [mm]

0

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0 1 2 3 4 5 6

shea

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ress

[

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shear displacement us [mm]

0

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2

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shea

rst

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[

MP

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shear displacement us [mm]

Result of computation

Laboratory test result

Result of computation

Laboratory test result

Result of computation

Laboratory test result

Result of computation

Laboratory test result

v = 0.002 mm/s

v = 0.000005 mm/s

N = 10 MPa

carnallitit

e

rock salt

N = 10 MPa

carnallitit

e

rock salt

σN=10 MPa

Page 12: 11 Testing Shear Strength and Deformation along Discontinuities in Salt

Minkley & Mühlbauer (2007) Test Results(Carnallite on salt)

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shea

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shear displacement us [mm]

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0 1 2 3 4 5 6

shea

rst

ress

[

MP

a]

shear displacement us [mm]

Result of computation

Laboratory test result

Result of computation

Laboratory test result

v = 0.002 mm/s

v = 0.000005 mm/s

0

2

4

6

8

10

12

0 1 2 3 4 5 6

shea

rst

ress

[

MP

a]

shear displacement us [mm]

0

2

4

6

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12

0 1 2 3 4 5 6

shea

rst

ress

[

MP

a]

shear displacement us [mm]

Result of computation

Laboratory test result

Result of computation

Laboratory test result

0

2

4

6

8

10

12

0 1 2 3 4 5 6

shea

rst

ress

[

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shear displacement us [mm]

0

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8

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shea

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[

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a]

shear displacement us [mm]

0

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0 1 2 3 4 5 6

shea

rst

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[

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a]

shear displacement us [mm]

0

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2

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shea

rst

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[

MP

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shear displacement us [mm]

Result of computation

Laboratory test result

Result of computation

Laboratory test result

Result of computation

Laboratory test result

Result of computation

Laboratory test result

v = 0.002 mm/s

v = 0.000005 mm/s

Test Results at

Two Different Shear VelocitiesSummary of Test Results

Page 13: 11 Testing Shear Strength and Deformation along Discontinuities in Salt

Testing/modeling options that can be considered

Measure composition of interface

Seam/interface may be modeled as contact surface, or as thin layer or one of more materials

Simple Mohr-Coulomb static/dynamic friction coefficient may be first approach

Select material models, parameters for shear stiffness & strength

Compare predictions of displacement along interface, change in aperture thickness, based on design, actual pressure application to measured values

Also consider including long-duration constant pressure, to collect measurements for transient, steady-state creep parameters

Measure permeability or flow in interface (and changes during test), if feasible

Ambient test required; additional heated test should be considered

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Page 14: 11 Testing Shear Strength and Deformation along Discontinuities in Salt

Proposed Slot Test in Salt (2018)

Alcove with horizontal clay seam, with “room divider” pillar created for test.

Slots cut in top, back of pillar; pressurized flatjacks installed to produced controlled normal, shear loading.

Measurements of applied pressure and displacement will capture the evolution of shear-induced characteristics of the inhomogeneity and neighboring salt during the test.

Pre-test analyses to predict changes to interface.

Other test configurations considered to eliminate bending moment.

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Page 15: 11 Testing Shear Strength and Deformation along Discontinuities in Salt

Proposed Slot Test in Salt

Proposed test alcove will look similar to YMP Busted Butte test shown below (pictures supplied by Los Alamos National Labs)

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Page 16: 11 Testing Shear Strength and Deformation along Discontinuities in Salt

Conclusion

Thank you!

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